In Re Water Rights of Deschutes River

294 P. 1049, 286 P. 563, 134 Or. 623, 1930 Ore. LEXIS 5
CourtOregon Supreme Court
DecidedMarch 6, 1929
StatusPublished
Cited by46 cases

This text of 294 P. 1049 (In Re Water Rights of Deschutes River) is published on Counsel Stack Legal Research, covering Oregon Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
In Re Water Rights of Deschutes River, 294 P. 1049, 286 P. 563, 134 Or. 623, 1930 Ore. LEXIS 5 (Or. 1929).

Opinions

BEAN, J.

A short history, as indicated in the briefs and record, relates that the Deschutes river is a nonnavigable stream and has well-defined banks and bed and flows directly north from Central Oregon. It is, perhaps, the longest and most important stream which, throughout its entire course, traverses the arid region of the state of Oregon. In the section through which this river flows there is no other source of water for most of the irrigated land.

The entire drainage area of the system is 9,180 square miles. The flow at the mouth fluctuates generally between 5,000 second feet and 8,000 second feet. Short time flood peaks do not usually exceed 16,000 second feet. The minimum flow over the land of the Columbia Deschutes Power company on the lower part of the river is approximately 4,500 second feet.

*630 Drainage Area

Deschutes river rises in the northern part of Klamath county, Oregon. Its drainage basin lies immediately east of the Cascade range, which the river parallels in its northerly course of nearly 200 miles to its confluence with the Columbia river. The arid and treeless portion of Central Oregon merges on the west into the less arid basin of the Deschutes, comprising about 9,000 square miles, in which the annual rainfall varies from about 10 inches along the main stream to as high as 100 inches at the crest of the Cascades, 30 miles westward. The upper portion of the drainage area, particularly to the south and west, is rough and mountainous and well forested. The agricultural lands consist largely of high table lands cut by deep canyons through which the river and its tributaries flow, and small areas of tillable land bordering the streams. The river is swift-flowing, especially in the lower portion where for a distance of over 100 miles it flows in a deep canyon. This portion of the stream is fed by large springs and important tributaries, and this fact, together with its unusual uniformity of flow makes the stream valuable for power development. Irrigation is essential for any material agricultural development in this region, although dry farming has been successful in some localities. The summer flow in the upper basin has practically all been appropriated for irrigation and other uses. Storage winterflow is possible in the upper portion of the basin. On the lower portion of the stream diversions for irrigation on a large scale are not feassible on account of the great elevation of the lands above the stream channels. The waters of the stream have as yet been only partially utilized for power, but there is a minimum flow of approximately 3,500 second feet available for this purpose when the entire flow of the river above is being diverted for irrigation.

*631 The Deschutes river is unlike any other stream in the state of Oregon in that the rise and fall does not exceed one foot from season to season, notwithstanding the fact that it has its source on the eastern slope of the Cascade mountains at the foot of the snow-capped peaks. There is a heavy run-off from the melting of the snows in the spring, yet on account of the porous condition of the territory through which the river flows, there is no perceptible rise in the river.

It developed in the adjudication that there were rights claimed for power purposes undeveloped, for power purposes developed, for irrigation and for domestic use and for stock water. As to the claims for power presently undeveloped on the lower stretches of the Deschutes river, the claimants stipulated priority in those who used the waters on the upper stretches of the river for irrigation.

Appeal oe Central Oregon Irrigation District

The Central Oregon Irrigation district is located on that part of the eastern Oregon plateau in which the soil consists of volcanic ash and throughout which there are numerous outcroppings of rock that have been through nature’s fire. The irrigation areas within the district are in patches and extend over a distance of 40 miles. There is a difference in elevation of the land of 700 feet within the district and climatic conditions are so different that the crop seasm is two weeks earlier in some portions of the district than in others. In the lower earlier sections, at the north end of the district, three cuttings of alfalfa hay may be obtained each year, while at the upper or south end of the district, but two cuttings are available.

The district is served by two canals, one leading almost directly north from the diversion works, known *632 as the Pilot Butte canal, the other branching in an easterly and northern direction known as the Central Oregon canal. One has a length of upwards of 40 miles; the other a length of upwards of 28 miles. Throughout this large area will be found some “made” soil, where there have been stream washes, etc., underlaid with gravel, and it is claimed this soil requires an unusual amount or low duty of water, even for this locality, while it is true of the entire district that because of the volcanic formation a large amount of water is required for the proper irrigation of crops.

The canals are constructed through volcanic rock, which is not water tight, resulting in a large seepage loss. These conditions make it impossible for the people living within the irrigation district to get their domestic or stock water from wells. Resort has been had to concrete cisterns, which must be filled at intervals with water from the irrigation ditches, thus presenting a serious question of adequate water supply for human beings and livestock during the winter season when water must be obtained at intervals when there is a flow of water "without freezing.

The Central Oregon Irrigation district’s claim is the successor in interest to the first effort to reclaim land on the Deschutes river under the Carey act. The rights claimed by claimant were initiated by the Pilot Butte Development company and the Oregon Irrigation company, to the rights of both, of which companies the Deschutes Irrigation and Power company succeeded in 1904. The latter company was succeeded by the Central Oregon Irrigation company in 1910.

On October 31, 1900, the Pilot Butte Development company posted on the banks of the Deschutes river, a short distance above what is now the city of Bend, *633 and duly filed a notice claiming 50,000 miner’s inches under a six-inch pressure, or approximately 1,250 cubic feet per second of the flow of the stream, and duly filed the notice on November 5,1900. At the same time at a point some distance down stream a similar notice was posted, in order that a diversion point might be preserved that would best serve the requirements disclosed by a survey. Rival claimants posted notices, and all of them applied for contracts to reclaim land under the Carey act. These claims were all eventually acquired by the Deschutes Irrigation and Power company, which was organized for the purpose and purchased the prior interests in 1904.

To constitute a valid appropriation of water three elements must always exist: (1) An intent to apply the water to some beneficial use existing at the time or contemplated in the future; (2) a diversion from the natural channel by means of a ditch, channel or other structure; and (3) the application of it within a reasonable timje to some useful purpose: Low v. Rizor,

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Bluebook (online)
294 P. 1049, 286 P. 563, 134 Or. 623, 1930 Ore. LEXIS 5, Counsel Stack Legal Research, https://law.counselstack.com/opinion/in-re-water-rights-of-deschutes-river-or-1929.